The rate of atmospheric carbon dioxide increase is currently 10 times faster than at any point in the past 50,000 years, research in Scotland and the US has shown.
A team of researchers led by Oregon State University and the University of St Andrews undertook a detailed chemical analysis of ancient Antarctic ice, revealing the stark findings and the impact of human emissions.
The findings, published in the Proceedings of the National Academy of Sciences (PNAS), provide important understanding of abrupt climate change periods in Earth’s past and offer insight into the potential impacts of climate change.
The rate of carbon dioxide (CO2) increase was branded “unprecedented”, and driven by human emissions.
When the gas enters the atmosphere, it contributes to warming of the climate due to the greenhouse effect.
In the past, the levels have fluctuated due to ice age cycles and other natural causes, but today they are rising because of human emissions, according to scientists.
Dr Kathleen Wendt, an assistant professor in Oregon State University’s College of Earth, Ocean, and Atmospheric Sciences (CEOAS) and the study’s lead author, said: “Studying the past teaches us how today is different. The rate of CO2 change today really is unprecedented.
“Our research identified the fastest rates of past natural CO2 rise ever observed, and the rate occurring today, largely driven by human emissions, is 10 times higher.”
Ice that built up in the Antarctic over hundreds of thousands of years includes ancient atmospheric gasses trapped in air bubbles.
Scientists used samples of ice, collected by drilling cores up to two miles deep to analyse the trace chemicals and build records of the climate in the past.
The US National Science Foundation supported the ice core drilling and the chemical analysis used in the study.
Previous research showed that during the last ice age, which ended about 10,000 years ago, there were several periods where carbon dioxide levels appeared to jump much higher than the average, but the measurements were not detailed enough to reveal the full nature of the rapid changes, limiting scientists’ ability to understand what was occurring.
Dr Wendt said: “You probably wouldn’t expect to see that in the dead of the last ice age.
“But our interest was piqued, and we wanted to go back to those periods and conduct measurements at greater detail to find out what was happening.”
Using samples from the West Antarctic Ice Sheet Divide ice core, Dr Wendt and colleagues investigated what was occurring during those periods, and identified a pattern that showed the jumps in carbon dioxide occurred alongside North Atlantic cold intervals known as Heinrich Events that are associated with abrupt climate shifts around the world.
Christo Buizert, an associate professor in the College of Earth, Ocean, and Atmospheric Sciences, and co-author of the study, said: “These Heinrich Events are truly remarkable. We think they are caused by a dramatic collapse of the North American ice sheet.
“This sets into motion a chain reaction that involves changes to the tropical monsoons, the Southern hemisphere westerly winds and these large burps of CO2 coming out of the oceans.”
Dr James Rae, from the School of Earth and Environmental Sciences at the University of St Andrews, and co-author of the study, said: “These Heinrich Events kick off an astonishing sequence of rapid shifts in climate around the world. They start with a weakening of the North Atlantic’s circulation system, which causes rapid cooling in NW Europe, sea ice expansion from Scotland to New York, and disruption to tropical monsoons.
“Our paper shows they also change winds and circulation in the ocean round Antarctica, which belches out CO2.”
During the largest of the natural rises, carbon dioxide increased by about 14 parts per million in 55 years, and the jumps occurred about once every 7,000 years or so – compared to current rates, when that magnitude of increase takes only five to six years.
Evidence suggests that during past periods of natural carbon dioxide rise, the westerly winds that play an important role in the circulation of the deep ocean were also strengthening, leading to a rapid release of CO2 from the Southern Ocean.
Other research has suggested that these westerlies will strengthen over the next century due to climate change.
The findings suggest that if that occurs, it will reduce the Southern Ocean’s capacity to absorb human-generated carbon dioxide, the researchers noted.
Dr Wendt said: “We rely on the Southern Ocean to take up part of the carbon dioxide we emit, but rapidly increasing southerly winds weaken its ability to do so.”
